The high-speed structure of the upper floors of the mantle of the Black Sea basin

Lateral velocity variations in the mantle lithosphere of the Black Sea basin down to the depth of 80 km were estimated from travel time residuals of P-waves recorded at the coastal stations from earthquakes within and around the Black Sea. The observed data were corrected for the crust structure tha...

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Bibliographic Details
Date:2011
Main Authors: Gobarenko, V. S., Yanovsky, T. B.
Format: Article
Language:rus
Published: Subbotin Institute of Geophysics of the NAS of Ukraine 2011
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/116929
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Journal Title:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal